Combining stereo‐video monitoring and physiological trials to estimate reef fish metabolic demands in the wild

Abstract Organismal metabolic rates (MRs) are the basis of energy and nutrient fluxes through ecosystems. In the marine realm, fishes are some of the most prominent consumers. However, their metabolic demand in the wild (field MR [FMR]) is poorly documented, because it is challenging to measure directly. Here, we introduce a novel approach to estimating the component of FMR associated with voluntary activity (i.e., the field active MR [AMRfield]). Our approach combines laboratory‐based respirometry, swimming speeds, and field‐based stereo‐video systems to estimate the activity of individuals. We exemplify our approach by focusing on six coral reef fish species, for which we quantified standard MR and maximum MR (SMR and MMR, respectively) in the laboratory, and body sizes and swimming speeds in the field. Based on the relationships between MR, body size, and swimming speeds, we estimate that the activity scope (i.e., the ratio between AMRfield and SMR) varies from 1.2 to 3.2 across species and body sizes. Furthermore, we illustrate that the scaling exponent for AMRfield varies across species and can substantially exceed the widely assumed value of 0.75 for SMR. Finally, by scaling organismal AMRfield estimates to the assemblage level, we show the potential effect of this variability on community metabolic demand. Our approach may improve our ability to estimate elemental fluxes mediated by a critically important group of aquatic animals through a non‐destructive, widely applicable technique.


| INTRODUC TI ON
Anthropogenic stressors, such as climate change, over-harvesting, and pollution, are affecting biological communities at an unprecedented rate (Halpern et al., 2008;Venter et al., 2016). Scientists and policy-makers are becoming increasingly concerned that these community impacts will irreversibly alter key ecosystem functions, preventing these natural systems from maintaining indispensable services to humans (Cardinale et al., 2012). In this context, tools to quantify and monitor ecosystem processes are valuable (Tilman et al., 2014). However, while there is a long-standing tradition in measuring ecological processes in mesocosms and controlled in situ experiments, the assessment of rates of ecological processes in natural conditions is still in its infancy (Reich et al., 2012), especially for marine ecosystems (Brandl, Rasher, et al., 2019).
In coastal marine ecosystems, fishes represent one of the most thoroughly studied, ecologically important, and economically valuable group of consumers (Bozec et al., 2004;Tamayo et al., 2018).
Despite the complexity of measuring the contribution of mobile species to ecosystem fluxes (Wilson et al., 2010), several attempts have been made to quantify the contributions of fishes to nutrient and carbon cycling (Brandl, Rasher, et al., 2019;Villéger et al., 2017).
These functions are usually quantified at the individual level, which can then be scaled up to community levels through an additive framework (Allgeier et al., 2014;Barneche et al., 2014;Brandl, Tornabene, et al., 2019;. While there are inherent limitations to this approach, individual-based modeling currently represents our best means to quantify ecological processes across communities of mobile, aquatic organisms. Nevertheless, the accuracy of these approaches inevitably depends on our capacity to precisely estimate the physiological requirements and expenditures of individuals in their natural environment. The metabolic rate (MR) of living organisms is an essential determinant of their physiological requirements and therefore represents a crucial parameter to estimate the flow of energy and nutrients in any ecosystem (Allen et al., 2005;Brown et al., 2004). MRs of fishes are generally evaluated through two metrics: (i) standard MR (SMR) (Fry, 1957;Vinberg, 1960), which corresponds to the MR of an inactive and fasting individual (Chabot et al., 2016) and (ii) maximum MR (MMR), which corresponds to the aerobic MR of an animal that is exercising at full capacity (Norin & Clark, 2016). Theory predicts that individual MR increases hypoallometric (sub-linearly) with body mass according to a power function with a scaling exponent of approximately 0.75 (Brown et al., 2004;Gillooly et al., 2001;West et al., 1997). While laboratory measurements of the SMR of resting fishes have both confirmed a scaling exponent close to 0.75 (Barneche et al., 2014;Clarke & Johnston, 1999) and rejected it (Bokma, 2004;Killen et al., 2016), an 0.75 scaling exponent has been used to estimate community-level MRs (Cheung et al., 2013;Deutsch et al., 2015;Holt & Jørgensen, 2015).
Knowledge of SMR and MMR allows for the calculation of a fish's aerobic scope, which is the ratio between MMR and SMR and represents the capacity to elevate MR above maintenance to support energetically demanding tasks such as physical activity and digestion (Clark et al., 2013). Within species, aerobic scope tends to increase with body mass regardless of being expressed in absolute (MMR minus SMR) or factorial (MMR divided by SMR) values (Halsey et al., 2018), as the scaling exponent of MMR is often observed to be higher than that of SMR (Glazier, 2005;Killen et al., 2007). Both SMR and MMR can be estimated relatively accurately in the laboratory through measurements of oxygen uptake rates (Clark et al., 2013;Svendsen et al., 2016). However, animals in the wild rarely reside at SMR or exercise maximally. Thus, calculations of energy expenditures in wild fishes are hamstrung by our inability to accurately estimate MRs in fishes that pursue their normal, daily activities in their natural environment.
The field MR (FMR) represents the average MR of an individual in the wild (Chung et al., 2019;Nagy, 2005) and lies somewhere between SMR and MMR (Nagy, 2005). On average, free-living fishes in their natural habitats will only exploit a given proportion of their aerobic scope and, in non-sedentary fishes, physical activity will be a major component of FMR (Chung et al., 2019). Thus, the factorial scope for activity (FSA), which corresponds to the ratio between the component of FMR related to physical activity (the AMR field ) and the SMR, is a better reflection of energy expenditure in the wild than the aerobic scope (Chung et al., 2019), bearing in mind that internal homeostatic processes such as digestion and reproduction also incur an energetic cost as part of the full FMR.
In terrestrial vertebrates, where the doubly labeled water technique has allowed for widespread quantification of FMR (Webster & Weathers, 1989), the metabolic scaling exponent of FMR tends to be higher than that of SMR (~0.8; Nagy, 2005). While the metabolic scaling exponent of MMR in fishes approximate or exceed 0.8 as well, the scaling of FMR or AMR field remains poorly documented important group of aquatic animals through a non-destructive, widely applicable technique.

K E Y W O R D S
activity, activity scope, field metabolic rate, fish, metabolic scaling, metabolism, swimming speed

T A X O N O M Y C L A S S I F I C A T I O N
Community ecology; Ecosystem ecology; Functional ecology; Movement ecology (Norin & Clark, 2016). Understanding how MR scales with body mass in the wild is fundamentally important for fisheries (e.g., stock assessments) and predictions of the effects of climate change, as the metabolic scaling exponent is an integral part of growth models used to forecast the size of fishes at both current and future temperatures (Von Bertalanffy, 1957;Cheung et al., 2013;Deutsch et al., 2015;Marshall & White, 2019).
Since FMR is challenging to measure for water-breathing animals in the aquatic environment (Treberg et al., 2016), it has only been estimated for a small number of fishes (e.g., Chung et al., 2019;Cruz-Font et al., 2016;Lucas et al., 1993;Murchie et al., 2011). These estimates are largely derived from biotelemetry approaches that rely on accelerometry tags and heart rate measurements calibrated with rates of oxygen uptake in the laboratory (Gräns et al., 2009;Treberg et al., 2016). A major limitation of biotelemetry is that its application is limited to large individuals as it requires surgical attachment or implantation of tags (Gräns et al., 2009). More recently, FMR has been estimated from the isotopic composition of carbon in fish otoliths (Chung et al., 2019). However, this approach relies on destructive sampling and the generality of the undoubtedly promising results are yet to be applied across a broad range of species. Thus, noninvasive methods to estimate FMR on many co-occurring fish species in the field are needed to better understand the contributions of fishes to ecosystem functioning.
Here, we propose a new approach to estimating a major component of the FMR, the AMR field . Specifically, we estimated the SMR and MMR of six reef fish species using traditional respirometry techniques in the laboratory, and then quantified in situ swimming speeds of the same species using underwater stereo-video systems.
This permitted us to derive AMR field and the FSA on the basis of the theoretical relationship between MR and swimming speed, and to assess the mass-scaling exponents of AMR field for each species. By combining our results with underwater visual census data of fish size and abundance on reefs around Mo′orea, French Polynesia, we also estimate assemblage-level SMR and AMR field . In doing so, we demonstrate the potential applicability of our approach to tackle questions across fields of organismal, community, and ecosystem ecology in the marine biome.

| Theory
Our approach to quantifying the AMR field is based on the relationship between swimming speed (v) and MR Norin & Clark, 2016;Torres & Childress, 1983) (Figure 1). We assume that MRs vary predictably with swimming speed following a traditional power function, which can be adapted to a log 10 transformed form (Brett, 1964;Korsmeyer et al., 2002): We further assume that (1) the SMR represents the MR of an individual when its swimming speed is zero and (2) the MMR represents the oxygen uptake rate of individuals at their maximum swimming speed (v max ; Figure 1). The previous equation can thus be rewritten as: and AMR field can then be estimated using the average swimming speed in the field (v field ): The FSA is computed by dividing a fish's AMR field by their SMR. We note that the FSA tends to be calculated over a 24 period, which means that we have to consider the amount of time spent resting. If a fish is resting for a certain amount of hours (t) a day and the MR at resting equals the SMR, the FSA can be estimated as follows: Thus, on the basis of known SMR and MMR estimates along with the v max of individuals, AMR field of a species can be estimated if the average swimming speed in the field (v field ) for specific body size is known. For our case study, we estimated SMR and MMR using respirometry in the laboratory, obtained v max through (1) MR = a10 bv (2) log 10 (MR) = log 10 (a) + bv, (3) log 10 (MR) = log 10 (SMR) + log 10 (MMR) − log 10 (SMR) v max v, (4) log 10 AMR field = log 10 (SMR) + log 10 (MMR) − log 10 (SMR) v max v field , (5) FSA = (24 − t)AMR field + tSMR 24SMR .

F I G U R E 1
Definition of fish metabolic rates along with the swimming speed range. SMR is the standard metabolic rate at swimming speed (v) zero. AMR field is field active metabolic rate at average swimming speed in the field (v field ). MMR is maximum metabolic rate, assumed to be reached at maximum swimming speed (v max ) empirical data available in the literature, and estimated v using stereo-camera video recordings in the field. We then used these estimates of AMR field to estimate the FSA and the metabolic scaling exponent for AMR field . Finally, to evaluate the impact of assessing assemblage-level MRs on the basis of a realistic proxy of FMR, AMR field (instead of using the more commonly measured SMR as an estimate of minimum energetic requirements), we scaled up our estimates at the assemblage level according to visual census data of fish sizes and abundances on a coral reef in Mo′orea, French Polynesia.

| Standard and maximum metabolic rates
To quantify SMR and MMR, we conducted intermittent-closed respirometry experiments (Clark et al., 2013;Steffensen, 1989) at 28 ± 0.5°C on a total of 68 individuals across the six study species with the sample size per species ranging between four and 23 individuals. After an acclimation and fasting period of 48 h in aquaria, the fish were individually transferred to a water-filled tub at 28°C and sequentially chased by the experimenter until visibly exhausted to elicit MMR (Norin & Clark, 2016). Once the chasing was concluded, each individual was immediately placed in a respirometry chamber submerged in an ambient and temperaturecontrolled tank, where they were left for approximately 24 h to reach SMR. The intermittent respirometry cycles consisted of a measurement (closed) period followed by an open period during which the respirometry chambers were flushed with fully aerated water from the ambient tank. Based on previous work (Norin & Clark, 2016), we considered the oxygen uptake rate (ṀO 2 ) during the first closed cycle (directly after transferring the fish) to be reflective of the individual's MMR. Depending on fish size, respirometry chambers ranged in volume (including tubes and pumps) from 0.38 to 4.4 L, and measurement and flush periods lasted between 2-9 and 3-5 min, respectively. SMR was calculated as the average of the 10% lowest Ṁ O 2 values measured during the entire respirometry trial, after the removal of outliers, while MMR was calculated from the slope of the first measurement period (Chabot et al., 2016).

| Field swimming speeds
We used two underwater stereo-video systems that were placed on the seafloor to record fish movements in the wild. Each video system consisted of two small action cameras (GoPro Hero5 Black), mounted 90 cm from each other at an angle of approximately 6°. This method allows three-dimensional (3D) measurements (Butail & Paley, 2012;Hughes & Kelly, 1996). To analyze the recorded videos, we used VidSync, an open-source Mac application providing accurate 3D measurements (Neuswanger et al., 2016), which allows for synchronization, calibration, and analysis of videos. We recorded calibration videos to correct for the nonlinear optical distortion of the images due to camera lenses and underwater housings, and to define the 3D coordinate system (x, y, z) used throughout the analyses. Errors in length measurements through video analysis increase with distance from the cameras (Neuswanger et al., 2016). Thus, for each underwater stereo-video system, we fitted a linear regression model describing the error in measurements as a function of their distance from the nearest camera, which we used to adjust all measurements of distances and fish lengths ( Figure 1). We recorded 20 stationary stereo videos between November 19, 2018 and December 12, 2018. Videos were recorded at 12-14 m depth on the reef slope at the Tiahura long-term monitoring site in Mo′orea (17°29′00.6″S, 149°54′20.9″W) and at five different time periods: 5:00-7:00, 8:00-10:00, 11:00-13:00, 14:00-16:00, and 17:00-18:00. Each recording lasted for ~1 to 1.5 h. We then took measurements during three 10 min sequences with intervals of 10 min that excluded the first 2 min to account for the presence of divers. We took measurements for all fishes visible in both cameras for 3-5 s during the three 10 min sequences. For each individual, fork length was measured three times from the videos as the straight-line distance between the fish's head and its tail fork, and three to five consecutive swimming speeds were measured as the distance the fish moved over 3-5 s. Final fish lengths and swimming speeds were then calculated as the mean of the repeated measurements.
In total, we recorded lengths and speeds for 634 individuals, with sample sizes per species ranging between 64 and 264 individuals.

| Maximum swimming speed
We assumed maximum swimming speeds (v max ) from previous work that estimated the swimming speed at which a fish becomes exhausted and stops swimming when it is exposed to regular incremental changes in speed in an experimental flume (Brett, 1964;Fulton, 2007). In the original work of Fulton (2007), the maximum swimming speeds of 192 individuals from five fish families and their corresponding lengths were measured, and these measurements were then used in the present study to relate maximum swimming speed with body size and caudal aspect ratio as a proxy for variations in swimming ability while accounting for the effect of fish family and body shape type. Caudal aspect ratio and body shape values were retrieved from Fishbase (Froese & Pauly, 2018).

| Data analysis
We quantified AMR field and FSA by combining multiple regression models, that describe the relationships between SMR and MMR with body mass, swimming speed (v), and maximum swimming speed (v max ; from Fulton, 2007) with body size. First, we used the respirometry data to fit a relationship between either SMR or MMR and body mass using a Bayesian hierarchical model, while accounting for the co-variation between MMR and SMR. We define the log 10 of SMR and MMR to be normally distributed with a mean ( ) and a standard deviation ( ) as follows: where i is the individual, j is the species, k is the type of MR (SMR or MMR), a is the global intercept of the regression; a j,k is the effect on the intercept for each species and type of MR, b is the global slope of log 10 (weight), and b j,k is the effect on the slope for each species and type of MR. We obtained the mean intercept and slope per species by summing global-and species-level parameters. We used an informative normal prior for the global slope exponent (i.e., metabolic scaling exponent) with an average of 0.75 and 0.1 as the standard deviation (West et al., 1997). For all other parameters, we used weakly informative priors (Burkner, 2017).
Second, using the data retrieved from the video analyses, we fitted a hierarchical Bayesian regression model for estimating fish swimming speed as a function of body length. We defined the log 10 transformation of swimming speed to be the student t-distributed with degrees of freedom ( ), mean ( ), and a standard deviation ( ).
The student's t-distribution was applied to build a robust regression, as our data includes outliers (Motulsky & Brown, 2006).
where v is the swimming speed, i is the individual, j is the species, a is the global intercept of the regression, a j is the effect on the intercept for each species, b is the global slope, and b j is the effect on the slope of each species. For each species, regression exponents were estimated by summing two effects of the model: the global parameter and the species-specific effect on the global parameter.
Thirdly, we fitted a similar model to predict maximum swimming speed in function of body length and aspect ratio using data extracted from Fulton (2007), including random effects of the interaction between family and body shape on the intercept and slope of body size.
where i is the individual, j is the interaction of family and body shape, a is the global intercept of the regression, a j is the effect on the intercept for each family and body shape, b is the global slope, b j is the effect on the slope for each family and body shape, and AR is the aspect ratio of the tail. Here, we also applied the Student's t-distribution and used general uninformative priors. We then used this model to estimate the maximum swimming speed of the species included in our study.

| FAS, AMR field , and FSA calculations
We estimated the factorial aerobic scope (FAS), AMR field , and FSA for the full-size range of all model species (per cm). To estimate the fish's FAS at each possible length, we first predicted their SMR and MMR by estimating their weight using the published length-weight relationship accessed through FishBase (Froese et al., 2014), and making predictions based on our model parameters. For each iteration of the prediction, we calculated FAS as FAS = MMR SMR (F. Fry, 1947;Killen et al., 2016). Finally, we summarized the FAS for each species at all sizes by taking means, standard deviations, and 95% credible intervals.
To estimate AMR field , we needed the SMR, MMR, v max , and v field (log 10 AMR field = log 10 (SMR) + log 10 (MMR) − log 10 (SMR) v max v field ). For each length and species, we estimated v field , v max , SMR, and MMR using the above-mentioned regression models. To incorporate an estimate of uncertainty, we included 1000 iterations for v field . For v max , SMR and MMR we used the median of the predicted values in this step.
Once we determined AMR field , we calculated FSA with the following equation: We repeated this for each iteration and then summarized FSA per species per size. We assumed that fish rested for 12 h (i.e., sleeping) (Marshall, 1972). As such, for all studied species, we assumed that they are active during the day and inactive during the night.

| Assemblage-level estimates
In 2016, reef fish communities were assessed across 13 sites on the outer fringing reef around Mo′orea using underwater visual censuses. During each census, a single diver swam along a 25 m transect and counted all fishes within a 2 m wide band. All fishes were identified to the species level and their total length was estimated to be the nearest 1 cm. Each transect covered an area of 50 m 2 , except Tiahura and Haapiti, which covered an area of 100 m 2 each. At each site, three transects were performed, except for Tiahura and Haapiti where four and two transects were performed, respectively. We extracted data for our model species from this database, which resulted in 802 individuals across the six species. Then, we quantified the SMR and AMR field for each individual using the above-mentioned methodology. Finally, we calculated the total SMR and AMR field of the fish assemblage composed of the six species at each site by summing across individual estimates.

| Standard and maximum metabolic rates
The regression model predicting MRs (log 10 of SMR and MMR) as a function of log 10 of body mass with varying slopes and intercepts per species had a Bayesian R 2 of .96 (Table 1; Figure 2). The average metabolic scaling exponent across species was 0.73 for SMR and 0.78 for MMR (Table 1). The median species-specific scaling exponents varied between 0.68 and 0.76 for SMR and between 0.77 and 0.78 for MMR.

| Swimming speed
The regression model predicting species-specific swimming speed as a function of body size had a median Bayesian R 2 of .57 and its residual variance ( ) was 0.37. The average species-specific slope values varied between 0.18 and 0.97 ( Figure 3, Table S2). At the individual scale, the 95% credible interval of swimming speed predictions varied between 28.5 and 32.4 cm s −1 across all species and size classes.
For maximum swimming speed, our model showed an increase in body size and aspect ratio (Table S3), with a median Bayesian R 2 of .46. We then used this model to estimate maximum swimming speeds ( Figure 3).

| FMR, FAS, and FSA estimations
We estimated AMR field , FAS, and FSA across the size range of our study species as observed in the monitoring dataset from Mo′orea in 2016. Across all species and size classes, the average AMR field estimates ranged between 0.001 and 1.013 g O 2 d −1 at the individual level (Table S4). FAS and FSA estimate range between 2.4 and 7.0, and between 1.2 and 3.2, respectively, across species and sizes. The scaling exponent of AMR field was higher than the SMR exponent for all species, except for C. striatus (Figure 4a), hence, FSA increased with size for all those species (Figure 4b). The scaling exponent of AMR field was considerably higher than the MMR exponents for N. lituratus and O. niger.

| Assemblage-level predictions
Scaling up SMR and AMR field to the assemblage level revealed major variation in the two estimates of metabolism, with average SMR (±SD) for this assemblage of six fish species across sites (ranging between 0.026 ± 0.009 and 0.325 ± 0.021 g O 2 m −2 d −1 ; Figure 5) tending to be about half total AMR field (ranging betwen 0.036 ± 0.014 and 0.465 ± 0.07 g O 2 m −2 d −1 ). Spatial variation in total SMR and AMR field reflected patterns in the relative abundance of the six study species across sites (Figures 5 and S4)

| DISCUSS ION
FMR is an essential organismal process that mediates consumption rates across the food web, thus influencing system-wide fluxes of energy and nutrients. By coupling laboratory data on MRs with field observations of body size and swimming activity through stereovideo analysis, we estimated the activity component of FMR (the AMR field ). Further, we demonstrate that the FSA of reef fish species varies substantially across species, and that the metabolic scaling exponent of AMR field can substantially exceed the canonical value of 0.75, which also affects community-level estimates of MR.
Therefore, our results highlight the potential pitfalls of estimating the community-level MR of heterogeneous reef fish assemblages based on scaled-up estimates of SMR instead of AMR field . We suggest that the coupling of physiological traits with stereo-video analyses provides an opportunity to estimate FMRs of fishes in marine environments that allow for visual assessments.
The FSA can be an important parameter to predict the energy consumption of fishes in the wild (e.g., Schiettekatte et al., 2020).
Our estimates of FSA were comparable to previous estimates for a small freshwater fish, in which the FSA was obtained through a combination of bioenergetic modeling and behavioral observations (~1.9; Trudel & Boisclair, 1996). In contrast, several other fish species may have a much higher AMR field as locomotion has been reported to increase MR up to fivefold, and up to ninefold in tuna (Thunnus albacares) (Brill & Bushnell, 1991;Chabot et al., 2016). However, it is still challenging to quantify where AMR field lies for most species.
The varying estimates of FSA may relate to the swimming speed and the aerobic capacity of the studied species (Clark et al., 2013;Killen et al., 2016). In our case study, the two fishes with the highest FSA were O. niger and C. argus, which appear to exploit about 45% and 60% of their aerobic scope in their natural environment, respectively. Therefore, C. argus has a high FSA mostly due to its high aerobic scope, while O. niger has the highest FSA in our case study both because of a high aerobic capacity and because it uses a larger proportion of it for swimming. On the other hand, fishes with a lower FSA (i.e., C. ornatissimus, C. striatus, and Z. scopas) were quite active, relative to their maximum swimming capacities, and exploited more F I G U R E 2 Linear regressions between log 10 -transformed metabolic rate (g O 2 d −1 ) and weight (g) for the study species. Symbols represent empirical measurements. Solid and dashed lines represent predicted mean standard metabolic rate (SMR) and maximum metabolic rate (MMR) values, respectively. Transparent areas are the 95% credible intervals of the fitted values of the regression F I G U R E 3 Linear regressions between log 10 -transformed speed (cm s −1 ) and length (cm) for the six study species. Symbols represent the raw data of individuals measured through stereovideo analysis. Solid lines and shaded areas represent the predicted mean back-transformed values, and associated 95% credible interval of swimming speeds. The dashed lines represent the predicted maximum swimming speeds than 50% of their aerobic scope. However, because their aerobic scope is low, so is their FSA.
These results corroborate the notion that AMR field in fishes is strongly influenced by ecological traits, such as size, trophic level, and habitat use (Brown et al., 2004;Killen et al., 2016;Nash et al., 2015). Larger fishes tend to have a higher aerobic capacity than smaller species (Brown et al., 2004;Killen et al., 2007), and larger sizes in fishes permit the establishment of larger home ranges (Nash et al., 2015). Furthermore, predators often have a higher metabolic capacity, compared to herbivores, and pelagic fishes often have higher metabolic potential than benthic fishes, as they have high locomotory demands because of their mobility in a 3D environment Nash et al., 2015). Pairwise comparisons among our study species (e.g., the herbivorous Z. scopas vs. the carnivorous C. argus or the benthopelagic C. striatus vs. the epipelagic O. niger) strongly support an ecological basis for metabolic differentiation.
Beyond interspecific differences, our results suggest that AMR field scales differently with body mass compared to SMR or MMR. The SMRs of our study species varied predictably with body mass, in accordance with the metabolic theory of ecology (Brown et al., 2004), with the average slope value approximating the allometric scaling exponent of 0.75 often found empirically and predicted theoretically by West et al. (1997) Importantly, there appears to be a higher interspecific variability of the scaling exponent for AMR field compared to that for SMR and MMR. This underlines the importance of both species identity and body size when estimating FMR.
Scaling up, community-level SMRs should vary predictively with both community composition and intraspecific size structure (Allen et al., 2005;Barneche et al., 2014). However, failing to account for the increased variation in scaling exponents of FMR may lead to severe underestimates of the contribution of large mobile fishes to the total respiration of fish communities. Indeed, comparing our assemblage-level estimates based on SMR with assemblagelevel estimates based on AMR field reveals the potential pitfalls of using SMR to study community-level MRs (e.g., Cheung et al., 2013;Deutsch et al., 2015;Holt & Jørgensen, 2015). The ratio between  (Fulton, 2007). Although we accounted for size, family, variation in body shapes, and a proxy for swimming ability, swimming speed across species within a family and body shape may still differ substantially, introducing potential bias to our calculations.
Further, our method relies on the assumption that MR varies predictably with swimming speed following a traditional power function (Brett, 1964;Korsmeyer et al., 2002). While this power function has been found to accurately predict MR for multiple species, more complex functions may be optimal for others, for example incorporating a plateau at the highest swimming speeds .
Finally, the method we used to define MMR (i.e., the chase method) could have introduced additional bias. MMR does not differ between post-exercise (e.g., chase) and sustained swimming across multiple species (Killen et al., 2017). However, there is alternative evidence from coral reef fishes suggesting that they can in fact achieve a higher maximum rate of oxygen uptake while swimming compared to after a chase Rummer et al., 2016). Future studies could resolve all of the above-mentioned issues by measuring swimming speed and respiration rate simultaneously in the laboratory and our approach can easily be adapted when additional data become available.
F I G U R E 4 (a) Fitted scaling exponents for standard metabolic rate (SMR), maximum metabolic rate (MMR), and field metabolic rate (AMR field ) based on slopes of the log 10 -log 10 relationships between the metabolic rates (g O 2 d −1 ) and body mass (g  Holt & Jørgensen, 2015). SDA can be measured in the laboratory, where a fish is given a meal and the resulting increase in oxygen consumption is measured for the duration of the digestion of this meal. SDA relates predictably to both the meal size and body mass of a fish (Secor, 2009), but using this relationship to calculate the SDA of species in natural communities is not feasible. It is nearly impossible to track the frequency of meals and meal sizes of fishes in the wild, even though some bioenergetic modeling allows for an approximation of daily consumption rates (e.g., Schiettekatte et al., 2020). Further, these experiments are largely based on predatory fishes, and do not necessarily represent natural feeding behavior as many fishes do not consume and digest a meal F I G U R E 5 Field (AMR field ) and standard metabolic rates (SMR) of an assemblage of six reef fish species at 13 sites around Mo′Orea, French Polynesia. Dashed lines represent 1.5 times the SMR as a reference. Colored bars display the relative abundances of the reef fish species at each site fully before eating the next meal. Notably, herbivores, detritivores, and planktivores, feed constantly, and their energy expenditure related to digestion is understudied. Therefore, we stress the need for more research on the energy consumption of digestion across a wide range of fishes to achieve improved FMR approximations for fish communities in the wild.
Despite these limitations, our proposed method may help us understand some of the variations in AMR field among reef fishes, which is necessary to understand ecosystem-level estimates of elemental fluxes. So far, the quantification of AMR field is limited to laboratory techniques that are reliant on destructive sampling (analysis of trace elements in otoliths; Chung et al., 2019), or restricted to species that are big enough to be tagged with biotelemetry equipment (Brodie et al., 2016;Treberg et al., 2016). When combined with respirometry trials, stereo-video offers a non-destructive and non-invasive alternative to these techniques that can be applied to all species that can be reliably observed using in situ cameras. While the post-hoc treatment of the stereo-video outputs demands significant time and effort, the development of open-source software to automate data collection from the video will greatly strengthen our ability and non-destructive approach to quantifying reef fish AMR field (Bassett & Montgomery, 2011;Guénard et al., 2008). writing -review and editing (equal).

ACK N OWLED G M ENTS
We thank the staff at CRIOBE, Moorea, for field support. Further, we would like to express gratitude to Camille Gache and Yann Lacube for their help in the field. Finally, we thank CRIOBE for sharing UVC data from their long-term monitoring program.

DATA AVA I L A B I L I T Y S TAT E M E N T
All data and code needed to reproduce results, tables, and figures are provided at https://github.com/nschi ett/activ ity_rate_fishes.

O PE N R E S E A RCH BA D G E S
This article has earned an Open Data badge for making publicly available the digitally-shareable data necessary to reproduce the reported results. The data is available at https://github.com/nschi ett/ activ ity_rate_fishes.